Search results for "Dynamic equation"

showing 10 items of 14 documents

Boulder coastal deposits at Favignana Island rocky coast (Sicily, Italy): Litho-structural and hydrodynamic control

2018

Boulders are frequently dislodged from rock platforms, transported and deposited along coastal zones by high-magnitude storm waves or tsunamis. Their size and shape are often controlled by the thickness of bedding planes as well as by high-angle to bedding fracture network. We investigate these processes along two coastal areas of Favignana Island by integrating geological data for 81 boulders, 49 rupture surfaces (called sockets) and fracture orientation and spacing with four radiocarbon dates, numerical hydrodynamic analysis, and hindcast numerical simulation data. Boulders are scattered along the carbonate platform as isolated blocks or in small groups, which form, as a whole, a disconti…

010504 meteorology & atmospheric sciencesBeddingSettore GEO/02 - Geologia Stratigrafica E SedimentologicaLithologyCarbonate platformSettore GEO/03 - Geologia StrutturaleStorm wave010502 geochemistry & geophysics01 natural sciencesHydrodynamic equationsBoulders; Fracture network; Hydrodynamic equations; Storm waves; Earth-Surface ProcessesBedBouldersGeomorphologyBoulder0105 earth and related environmental sciencesEarth-Surface ProcessesBoulders.Fracture network Hydrodynamic equations Storm wavesBermStorm wavesStormHydrodynamic equationClastic rockFracture (geology)Fracture networkFracture network;Storm waves;Boulders;Hydrodynamic equationsGeology
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A reexamination of the equilibrium conditions in the theory of water drop nucleation

1975

The thermodynamic equations necessary to describe the conditions for equilibrium between a highly curved surface of a liquid and its vapour are re-examined. The complete equilibrium behaviour is reduced to one single differential equation for each component in an arbitrary c -component system. It is shown that this general formulation can be specialized to describe the conditions for equilibrium between water vapour and a pure water drop, the drop carrying an electric charge, containing a water soluble substance and/or containing a water insoluble nucleus. In the light of the present formulation, some incorrect physical statements of treatments by various authors reported in literature are …

Atmospheric ScienceMaterials science010504 meteorology & atmospheric sciencesDifferential equationEquilibrium conditionsDrop (liquid)NucleationThermodynamicsGeneral MedicineWater insolubleThermodynamic equationsOceanographyElectric charge01 natural sciencesWater vapor0105 earth and related environmental sciencesTellus A
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A method for the investigation of high-order two-frequency asynchronous oscillators

1992

A general method for analysing asynchronous high-order two-frequency oscillators is presented. the oscillator model is made up of a GC non-linear parallel group embedded in a linear lumped time-invariant network of any order. the approach devised rests on the identification of a pair of narrow-band impedance operators which permit one to derive first-approximation steady state and dynamic equations in the phasor domain—as well as stability criteria—in a simple and expressive manner. Previous results from averaging and perturbation treatments on fourth-order asynchronous oscillators are shown to be obtainable from this theory as particular cases. the sixth-order oscillator chosen as an appli…

General methodControl theoryAsynchronous communicationApplied MathematicsPhasorPerturbation (astronomy)Electrical and Electronic EngineeringHigh orderDynamic equationElectrical impedanceComputer Science ApplicationsElectronic Optical and Magnetic MaterialsMathematicsInternational Journal of Circuit Theory and Applications
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Water-Hydrophobic Zeolite Systems

2012

Water intrusion-extrusion in hydrophobic microporous AFI, IFR, MTW and TON pure silica zeolites (zeosils) has been investigated through molecular dynamics (MD) simulations. It was found that intruded water volumes correlate with the free volume of the zeosil unit cells. Calculated adsorption isotherms allowed us to estimate the amounts of water intruded, and deviations from experiments (lower experimental with respect to calculated intrusion pressures) have been;explained in terms of connectivity defects in the synthesized materials. Water phase transitions in defectless zeosils occur in a narrow range at high pressure. On the basis of a simple model, we derived a thermodynamic equation tha…

Phase transitionProperties of waterADSORPTIONThermodynamicsALPO4-5SSZ-24Thermodynamic equationsITQ-4 IFRMolecular dynamicschemistry.chemical_compoundAdsorptionComputational chemistryPhysical and Theoretical ChemistryZeoliteSILICALITE-1 ZEOLITEChemistryMicroporous materialDEFECTSMOLECULAR-DYNAMICS SIMULATIONSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsGeneral EnergyVolume (thermodynamics)STATISTICAL-MECHANICSMONTE-CARLO SIMULATIONSINTRUSION
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Fractional-Order Thermal Energy Transport for Small-Scale Engineering Devices

2014

Fractional-order thermodynamics has proved to be an efficient tool to describe several small-scale and/or high-frequency thermodynamic processes, as shown in many engineering and physics applications. The main idea beyond fractional-order physics and engineering relies on replacing the integer-order operators of classical differential calculus with their real-order counterparts. In this study, the authors aim to extend a recently proposed physical picture of fractional-order thermodynamics to a generic 3D rigid heat conductor where the thermal energy transfer is due to two phenomena: a short-range heat flux ruled by stationary and nonstationary transport equations, and a long-range thermal …

PhysicsFundamental thermodynamic relationbusiness.industryMechanical EngineeringNon-equilibrium thermodynamicsThermodynamic equationsThermodynamic systemThermodynamic free energyLong-range energy transport Fractional calculus Phonons transport Fractional heat transfer Kapitza effectStatistical physicsSettore ICAR/08 - Scienza Delle CostruzionibusinessTransport phenomenaThermal energyThermodynamic processJournal of Nanomechanics and Micromechanics
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Zur Frage der Charakterisierung stationärer Bewegungen in der Hydrodynamik

1958

Helmholtz andKorteweg propose that the steady motion of a viscous fluid under constant extraneous forces having a single-valued potential dissipates—for any given region and assuming that inertia terms in the dynamic equations can be neglected—less energy than any other motion with the same values of velocity at the boundary.—A generalization of this proposition is here given, and an application discussed. The application deals with the motion of a simple macromolecule model in an inhomogeneous field of flow—a motion caused only by the influence ofStokes' friction.

PhysicsGeneralizationApplied MathematicsGeneral Mathematicsmedia_common.quotation_subjectGeneral Physics and AstronomyMotion (geometry)MechanicsViscous liquidInertiasymbols.namesakeClassical mechanicsHelmholtz free energyInhomogeneous fieldsymbolsConstant (mathematics)Dynamic equationmedia_commonZeitschrift für angewandte Mathematik und Physik ZAMP
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The relaxation-time limit in the quantum hydrodynamic equations for semiconductors

2006

Abstract The relaxation-time limit from the quantum hydrodynamic model to the quantum drift–diffusion equations in R 3 is shown for solutions which are small perturbations of the steady state. The quantum hydrodynamic equations consist of the isentropic Euler equations for the particle density and current density including the quantum Bohm potential and a momentum relaxation term. The momentum equation is highly nonlinear and contains a dispersive term with third-order derivatives. The equations are self-consistently coupled to the Poisson equation for the electrostatic potential. The relaxation-time limit is performed both in the stationary and the transient model. The main assumptions are…

PhysicsIndependent equationApplied MathematicsGlobal relaxation-time limitQuantum hydrodynamic equationsEuler equationsMomentumNonlinear systemsymbols.namesakeClassical mechanicsThird-order derivativesMaster equationQuantum drift–diffusion equationssymbolsMethod of quantum characteristicsPoisson's equationQuantum dissipationAnalysisJournal of Differential Equations
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XVII.Thermodynamic principle governing stationary states

1933

(1933). XVII. Thermodynamic principle governing stationary states. The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science: Vol. 16, No. 104, pp. 248-263.

PhysicsThermodynamicsThermodynamic equationsThermodynamic systemStationary stateMathematical physicsThe London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science
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Hydrodynamic equations of anisotropic, polarized and inhomogeneous superfluid vortex tangles

2008

We include the effects of anisotropy and polarization in the hydrodynamics of inhomogeneous vortex tangles, thus generalizing the well known Hall-Vinen-Bekarevich-Khalatnikov equations, which do not take them in consideration. These effects contribute to the mutual friction force ${\bf F}_{ns}$ between normal and superfluid components and to the vortex tension force $\rho_s{\bf T}$. These equations are complemented by an evolution equation for the vortex line density $L$, which takes into account these contributions. These equations are expected to be more suitable than the usual ones for rotating counterflows, or turbulence behind a cylinder, or turbulence produced by a grid of parallel th…

PhysicsTurbulenceCondensed Matter::OtherFOS: Physical sciencesStatistical and Nonlinear PhysicsTourbillonCondensed Matter PhysicsPolarization (waves)VortexCylinder (engine)law.inventionSuperfluidityPhysics::Fluid DynamicsCondensed Matter - Other Condensed MatterClassical mechanicslawEvolution equationAnisotropySettore MAT/07 - Fisica MatematicaSuperfluid turbulence Liquid helium II Hydrodynamic equationsOther Condensed Matter (cond-mat.other)
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Relative importance of second-order terms in relativistic dissipative fluid dynamics

2014

[Introduction] In Denicol et al. [Phys. Rev. D 85 , 114047 (2012)], the equations of motion of relativistic dissipative fluid dynamics were derived from the relativistic Boltzmann equation. These equations contain a multitude of terms of second order in the Knudsen number, in the inverse Reynolds number, or their product. Terms of second order in the Knudsen number give rise to nonhyperbolic (and thus acausal) behavior and must be neglected in (numerical) solutions of relativistic dissipative fluid dynamics. The coefficients of the terms which are of the order of the product of Knudsen and inverse Reynolds numbers have been explicitly computed in the above reference, in the limit of a massl…

Physics::Fluid Dynamicsextended irreversible thermodynamicskinetic-theoryhydrodynamic equationsderivoiminenjärjestelmätrenormalization-group methodNonlinear Sciences::Cellular Automata and Lattice Gasesmoment method
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